Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Michal Poňavič"'
Publikováno v:
Geoscience Research Reports. :17-20
Magnetostatic susceptibility of single crystals of graphite is negative (the mineral is diamagnetic) and strongly anisotropic. The in-phase component of dynamic susceptibility (measured in alternating magnetic field) is also negative, but an order-of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8414b6b3748f12c9a86075f264133db0
https://doi.org/10.5194/egusphere-egu21-2385
https://doi.org/10.5194/egusphere-egu21-2385
Autor:
František Hrouda, Jan Franěk, Stuart Gilder, Martin Chadima, Josef Ježek, Štěpánka Mrázová, Michal Poňavič, Martin Racek
Publikováno v:
Journal of Structural Geology. 154:104491
Literature data on single crystals of graphite shows that this mineral is diamagnetic and strongly anisotropic. In addition, it possesses high electrical conductivity and extremely strong conductivity anisotropy. The AC magnetic susceptibility of gra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba2a824905583db43b83272ea8430dfe
https://doi.org/10.5194/egusphere-egu2020-2868
https://doi.org/10.5194/egusphere-egu2020-2868
Publikováno v:
Journal of Geochemical Exploration. 187:118-130
New geochemical mapping results from the central part of Prague agglomeration are presented. The study is part of the EuroGeoSurveys Geochemistry Expert Group's ‘Urban Geochemistry’ (URGE) project. The aim of the project is to study and compare t
Publikováno v:
Geoscience Research Reports. :127-129
Publikováno v:
Environmental Earth Sciences. 77
The measurements of radon concentration and gamma dose rate across the detected, mylonitized and assumed faults were performed on 79 profiles situated in metamorphic, magmatic and sedimentary rocks of the Bohemian Massif. At each profile, 10 points (
Publikováno v:
Geoscience Research Reports.
Publikováno v:
Geoscience Research Reports.
Autor:
Michal Poňavič, Magdalena Zimová, Zdeňka Wittlingerová, Tereza Jandová, Ilja Knésl, Karel Dušek
Publikováno v:
Geoscience Research Reports.